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Lake water volume fluctuations in response to climate change in Xinjiang, China from 2002 to 2018
Author(s) -
Adilai Wufu,
Hongwei Wang,
Yun Chen,
Yusufujiang Rusuli,
Ligang Ma,
Shengtian Yang,
Zhang Fei,
Dan Wang,
Qian Li,
Yinbo Li
Publication year - 2020
Publication title -
peerj
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.927
H-Index - 70
ISSN - 2167-8359
DOI - 10.7717/peerj.9683
Subject(s) - altitude (triangle) , climate change , environmental science , physical geography , arid , latitude , snow , hydrology (agriculture) , glacial lake , water cycle , effects of high altitude on humans , water level , surface water , climatology , geography , glacier , ecology , geology , oceanography , meteorology , geometry , mathematics , geotechnical engineering , geodesy , cartography , environmental engineering , biology
Climate change has a global impact on the water cycle and its spatial patterns, and these impacts are more pronounced in eco-fragile regions. Arid regions are significantly affected by human activities like farming, and climate change, which influences lake water volumes, especially in different latitudes. This study integrates radar altimetry data from 2002 to 2018 with optical remote sensing images to analyze changes in the lake areas, levels, and volumes at different altitudes in Xinjiang, China. We analyzed changes in lake volumes in March, June, and October and studied their causes. The results showed large changes in the surface areas, levels, and volumes of lakes at different altitudes. During 2002–2010, the lakes in low- and medium-altitude areas were shrinking but lakes in high altitude areas were expanding. Monthly analysis revealed more diversified results: the lake water levels and volumes tended to decrease in March (−0.10 m/year, 37.55×10 8 m 3 ) and increase in June (0.03 m/year, 3.48×10 8 m 3 ) and October (0.04 m/year, 26.90×10 8 m 3 ). The time series lake water volume data was reconstructed for 2011 to 2018 based on the empirical model and the total lake water volume showed a slightly increasing trend during this period (71.35×10 8 m 3 ). We hypothesized that changes in lake water at high altitudes were influenced by temperature-induced glacial snow melt and lake water in low- to medium-altitude areas was most influenced by human activities like agricultural irrigation practices.

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